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ORE-LOCALIZING AND ORE-PRESERVING FACTOR OF LIGHTENING OF THE ORE-BEARING ALLUVIAL SEDIMENTS IN THE URANIUM DEPOSITS OF THE KHIAGDA ORE FIELD
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The throughout lightening up to the whitening of basement granites, ore-bearing alluvial sediments, volcanogenic-sedimentary strata and fracture zones of plateau basalts are shown on an example of Vershinnoye uranium ore deposit of Khiagda ore field of Vitimskiy uranium ore region. The contribution of deep carbonated waters with high reducing capacity to this process is shown. The ore-localizing and ore-preserving role of the ore-bearing alluvial sediments lightening process is proofed. The key similarities and differences of young (Vitim type) and ancient (Dalmatov type) paleovalley deposits in contrast to the classical bedded-infiltration deposits of the Tien Shan uranium megaprovince are shown.
Title: ORE-LOCALIZING AND ORE-PRESERVING FACTOR OF LIGHTENING OF THE ORE-BEARING ALLUVIAL SEDIMENTS IN THE URANIUM DEPOSITS OF THE KHIAGDA ORE FIELD
Description:
The throughout lightening up to the whitening of basement granites, ore-bearing alluvial sediments, volcanogenic-sedimentary strata and fracture zones of plateau basalts are shown on an example of Vershinnoye uranium ore deposit of Khiagda ore field of Vitimskiy uranium ore region.
The contribution of deep carbonated waters with high reducing capacity to this process is shown.
The ore-localizing and ore-preserving role of the ore-bearing alluvial sediments lightening process is proofed.
The key similarities and differences of young (Vitim type) and ancient (Dalmatov type) paleovalley deposits in contrast to the classical bedded-infiltration deposits of the Tien Shan uranium megaprovince are shown.
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